Agritrop
Accueil

Impact of roots, microorganisms and microfauna on the fate of soil phosphorus in the rhizosphere

Hinsinger Philippe, Herrmann Laetitia, Lesueur Didier, Robin Agnès, Trap Jean, Waithaisong Kittima, Plassard Claude. 2015. Impact of roots, microorganisms and microfauna on the fate of soil phosphorus in the rhizosphere. In : Phosphorus metabilism in plants. Plaxton William C. (ed.), Lambers Hans (ed.). Chichester : Wiley-Blackwell, 377-407. (Annual plant reviews, 48) ISBN 978-1-118-95885-8

Chapitre d'ouvrage ; Article de recherche
[img] Version publiée - Anglais
Accès réservé aux personnels Cirad
Utilisation soumise à autorisation de l'auteur ou du Cirad.
Chapitre final Hinsinger et al. 2015 Book chpt 13 Ann Plant Rev.pdf

Télécharger (1MB) | Demander une copie

Résumé : Phosphorus (P) occurs at low concentrations in soils because of the numerous processes responsible for P sorption or immobilisation. Soil P is also characterised by its restricted mobility, and thus the most limiting step of P acquisition is not its absorption by plant roots, but rather the many processes that determine the fate of soil P in the rhizosphere. This chapter describes these various processes, including those directly mediated by plants (which vary considerably with plant species), and those related to soil microbial and microfaunal activities. In order to overcome the restricted mobility of soil P, plants have evolved several features aimed at increasing the rhizosphere volume by increasing the absorptive surfaces, notably root elongation and branching. The formation of root hairs and mycorrhizas is also triggered by interactions with plant growth promoting microorganisms. Plants have also evolved strategies aimed at increasing soil P concentrations via the mobilisation of inorganic and organic pools of soil P. These imply changes in pH, and the release of P-mobilising compounds such as carboxylates and phosphatases, that are exuded by the roots themselves or by rhizosphere microorganisms. Finally, the soil microfauna (especially the predators of bacteria and fungi) play an important role in the cycling of soil P in the rhizosphere that deserves further consideration.

Mots-clés Agrovoc : nutrition des plantes, phosphore, rhizosphère, transport des substances nutritives, microbiologie, micro-organisme du sol, racine, enracinement, morphologie végétale, mycorhization, ectomycorhize, minéralisation

Mots-clés complémentaires : Architecture végétale

Classification Agris : F61 - Physiologie végétale - Nutrition
P34 - Biologie du sol
F60 - Physiologie et biochimie végétale
P33 - Chimie et physique du sol

Champ stratégique Cirad : Axe 1 (2014-2018) - Agriculture écologiquement intensive

Auteurs et affiliations

  • Hinsinger Philippe, INRA (FRA)
  • Herrmann Laetitia, Deakin University (AUS)
  • Lesueur Didier, CIRAD-PERSYST-UMR Eco&Sols (THA) ORCID: 0000-0002-6694-0869
  • Robin Agnès, CIRAD-PERSYST-UMR Eco&Sols (BRA)
  • Trap Jean, IRD (FRA)
  • Waithaisong Kittima, INRA (FRA)
  • Plassard Claude, INRA (FRA)

Autres liens de la publication

Source : Cirad-Agritrop (https://agritrop.cirad.fr/578914/)

Voir la notice (accès réservé à Agritrop) Voir la notice (accès réservé à Agritrop)

[ Page générée et mise en cache le 2024-10-27 ]